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Title: Origin of gilsonite fractures in Uinta basin, Utah

Conference · · Am. Assoc. Pet. Geol., Bull.; (United States)
OSTI ID:5589818

The concept of gilsonite fracture and vein evolution is still, by nature, a theoretical argument. A historical review presented with recent observations and conclusions divides this period of origin into five stages of formation. The Uncompahgre uplift established an initial ancestral pattern of northwest-trending anticlinal structures. These propagated northeastward throughout the Uinta and Piceance basins as a result of compression during the Pennsylvanian Period. Planes of weakness were imprinted vertically along the axes of these folds and subsequently affected the overlying Mesozoic sediments. Next, the Uinta uplift reenforced these northwest-trending folds and planes of weakness during the early Laramide orogeny. The third stage of formation involves contemporaneous deposition of Eocene sediments, including the kerogen of the Green River Formation. Differential compaction during diagenesis, over the northwest-trending residual highs formulated subperpendicular, localized tensile stresses. Vertical fractures propagated rapidly in an en echelon fashion along the imprinted axial planes of weakness. In the fourth stage of formation, fractures penetrated overlying reservoir intervals, which contained various combinations of liquid hydrocarbons and connate water. Released fluids entered the low-pressure voids and spread laterally and vertically throughout the Eocene sediments. A final period of inspisation and/or metamorphosis quickly altered the various liquid hydrocarbon deposits to form gilsonite and other bitumens. The variation of these bitumens is dependent on the original chemical composition of the individual reservoir zones during deposition.

Research Organization:
Utah Division Oil, Gas and Mining, Salt Lake City, UT
OSTI ID:
5589818
Report Number(s):
CONF-8408161-
Journal Information:
Am. Assoc. Pet. Geol., Bull.; (United States), Vol. 68:7; Conference: Energy and More in '84, Salt Lake City, UT, USA, 27 Aug 1984
Country of Publication:
United States
Language:
English